Official Series Description


Lab Data Summary

Aggregate lab data for the TEGURO soil series. This aggregation is based on all pedons with a current taxon name of TEGURO, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to TEGURO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
2781P04081980NV001008Teguro6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5740556,-118.2565278
2781P04011980NV001018Teguro7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5738056,-118.2565278

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TEGURO soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the TEGURO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the TEGURO series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the TEGURO series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with TEGURO share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the TEGURO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the TEGURO series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TEGURO, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

No block diagrams are available.

Map Units

Map units containing TEGURO as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Punchbowl-Teguro-Sumine association209110480479100j2jvnv76819851:63360
Jung-Newpass-Teguro association38434115479247j2plnv76819851:63360
Punchbowl-Jung-Teguro association20882570479097j2jrnv76819851:63360
Teguro-Rubble land-Punchbowl association31702275479202j2n4nv76819851:63360
Jobpeak-Teguro-Rock outcrop association300018488475254hyjsnv76919861:24000
Jobpeak-Teguro-Rock outcrop association97036695476697j01bnv77019951:24000
Teguro-Colbar-Cleavage association8606425476680j00snv77019951:24000
Itca-Teguro-Rock outcrop association80504702477022j0ctnv77419851:24000
Punchbowl-Teguro-Sumine association20915610479525j2zknv77519851:24000
Coztur-Teguro-Punchbowl association40934395479670j347nv77519851:24000
Teguro-Anatone complex, 2 to 20 percent slopes4404AO733385288jgnlor62620181:24000
Merlin-Teguro complex, very stony, 2 to 20 percent slopes20319470490587jghdor62819971:24000
Teguro very cobbly loam, 2 to 20 percent slopes32117674490746jgnjor62819971:24000
Merlin-Teguro complex, 2 to 15 percent slopes20212290490586jghcor62819971:24000
Teguro very stony loam, thin surface, 2 to 20 percent slopes3228450490747jgnkor62819971:24000
Teguro-Ateron complex, 2 to 20 percent slopes3244741490749jgnmor62819971:24000
Observation-Teguro complex, 2 to 20 percent slopes2433392490640jgk3or62819971:24000
Merlin-Erakatak-Teguro complex, 2 to 20 percent slopes1982299490576jgh1or62819971:24000
Anatone-Teguro-Observation complex, 2 to 20 percent slopes92225490968jgwpor62819971:24000
Teguro-Anatone complex, 2 to 20 percent slopes3231992490748jgnlor62819971:24000
Teguro gravelly loam, 5 to 20 percent slopes3201510490745jgnhor62819971:24000
Anatone-Teguro-Rock outcrop association, 2 to 40 percent slopes12846490483jgd1or62819971:24000
Teguro-Carryback complex, 5 to 20 percent slopes635791416901351tqqhor63520061:24000
Teguro gravelly loam, 5 to 20 percent slopes623635516901231tqq3or63520061:24000
Teguro cobbly loam, 2 to 20 percent slopes622213916901221tqq2or63520061:24000
Teguro-Anatone complex, 2 to 10 percent slopes253518185771020c34or6541:24000
Teguro-Cadlebutte complex, 2 to 15 percent slopes25177185770920c33or6541:24000

Map of Series Extent

Approximate geographic distribution of the TEGURO soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .